rabii; :3. Arr.crrii/.iji ■:.-.ria.' /-.'j^fj" vrrjn '!^ltl-i_i_i /r^j_uta_\oija •jrac i Ij^ Co.Tiniuni ty T/ps Sita D:'scriDnon 



■januy lou/is; 6. fine Siiitly loaiiis 

 3.' silty cifiy loan;; i6i (,idy loams 



SOIL TLxnj,-L- .. -^anuy lou/is; 6. fine Sci-nly lodiiis; 45% loaus; 23''i silt ;oani3; 



iLOPE-SLOPE ASPECT 



■■■ej" : X = -O.O i 



Standard deviation: 5 =; rj.Of, 



R.iiige: - ').. ^ -0.9 



Sites nauing: 



Positive slope-siope asp'.^ct values: 1""' 



Slope-slope aspect v.ilues jf 0: 29:; 



'legativg s lope-s ! upa aspect values: 54' 



SLOPE 



Mean: 



Stanoara d.iviation: 



.< ^ 2.0' 



'..0^ 



gOjI ZOrnVL CO;iFinURAiIO ^j__^^^^ T^. convex ;_57:^raiqht,^_2 :^ un.i,Ma ting; 2V concave 



SLOPE POSITION: 



■ 1 i?. ' .. bo-ut -a: — i£^ 1 ni-r, '': .-miA:. 7- i;nnpi- 



GPj^ZI;;g PPESSUR:- 'l.l-^qnt; 4.: I ight-iiinderate; 52,. moderate; 4', moderate high; 



DISTANCE TO STOCK WATER 



i'tedn: 



Stancird deviation: 



0.1 mi :i).5 kn) 



S = 0.4 ini (0.6 km) 



Arca/Agsm/Bogr c.t. is most often found in coulees, swales and on flats 

 above creeks. The extra moisture and protection afforded by such sites tend 

 to discount the importance of a slope-slope aspect calculation. Furthermore, 

 the horizontal configuration of large flat bottom coulees is straight (and 

 was so recorded) although the coulee itself is of course concave. These sites 

 receive more moisture than most Agsm-Bogr c.t. sites, and soils are heavier on 

 the average. 



57 



